Talo A, Stern M D, Spurgeon H A, Isenberg G, Lakatta E G
Laboratory of Cardiovascular Science, National Institute of Aging, National Institutes of Health, Baltimore, Maryland 21224.
J Gen Physiol. 1990 Nov;96(5):1085-103. doi: 10.1085/jgp.96.5.1085.
Single rat ventricular myocytes, voltage-clamped at -50 to -40 mV, were depolarized in small steps in order to define the mechanisms that govern the increase in cytosolic [Ca2+] (Cai) and contraction, measured as a reduction in myocyte length. Small (3-5 mV), sustained (seconds) depolarizations that caused a small inward or no detectable change in current were followed after a delay by small (less than 2% of the resting length), steady reductions in cell length measured via a photodiode array, and small, steady increases in Cai measured by changes in Indo-1 fluorescence. Larger (greater than -30 and less than -20 mV), sustained depolarizations produced phasic Ca2+ currents, Cai transients, and twitch contractions, followed by a steady current and a steady increase in Cai and contraction. Nitrendipine (or Cd, verapamil, or Ni) abolished the steady contraction and always produced an outward shift in steady current. The steady, nitrendipine-sensitive current and sustained increase in Cai and contraction exhibited a similar voltage dependence over the voltage range between -40 and -20 mV. 2 microM ryanodine in the presence of intact Ca2+ channel activity also abolished the steady increase in Cai and contraction over this voltage range. We conclude that when a sustained depolarization does not exceed about -20 mV, the resultant steady, graded contraction is due to SR Ca2+ release graded by a steady ("window") Ca2+ current. The existence of appreciable, sustained, graded Ca2+ release in response to Ca2+ current generated by arbitrarily small depolarizations is not compatible with any model of Ca2(+)-induced Ca2+ release in which the releasing effect of the Ca2+ channel current is mediated solely by Ca2+ entry into a common cytosolic pool. Our results therefore imply a distinction between the triggering and released Ca2+ pools.
将单个大鼠心室肌细胞钳制在-50至-40 mV电压下,以小步幅进行去极化,目的是确定调控胞质[Ca2+](Cai)增加和收缩的机制,收缩以肌细胞长度的缩短来衡量。小幅度(3-5 mV)、持续(数秒)的去极化导致小的内向电流或未检测到电流变化,延迟后,通过光电二极管阵列测量到细胞长度出现小幅度(小于静息长度的2%)、稳定的缩短,同时通过Indo-1荧光变化测量到Cai出现小幅度、稳定的增加。较大幅度(大于-30 mV且小于-20 mV)、持续的去极化产生了阶段性的Ca2+电流、Cai瞬变和抽搐收缩,随后是稳定电流以及Cai和收缩的稳定增加。尼群地平(或镉、维拉帕米或镍)消除了稳定收缩,并且总是使稳定电流向外偏移。在-40至-20 mV的电压范围内,稳定的、对尼群地平敏感的电流以及Cai和收缩的持续增加表现出相似的电压依赖性。在完整的Ca2+通道活性存在的情况下,2 microM的ryanodine也消除了该电压范围内Cai和收缩的稳定增加。我们得出结论,当持续去极化不超过约-20 mV时,所产生的稳定的、分级的收缩是由于SR Ca2+释放由稳定的(“窗口”)Ca2+电流分级所致。响应任意小的去极化产生的Ca2+电流而存在可观的、持续的、分级的Ca2+释放,这与任何Ca2(+)-诱导的Ca2+释放模型均不相符,在这些模型中,Ca2+通道电流的释放作用仅由Ca2+进入共同的胞质池介导。因此,我们的结果意味着触发Ca2+池和释放Ca2+池之间存在区别。